Abstract
The very first studies of the Noril’sk deposits were launched by N. N. Urvantsev in 1919, and these deposits have now been studied for almost one century. During these years, the unique ores of the Talnakh and Oktyabr’skoe deposits were discovered. Their resources, composition, and mineralogical diversity have no equivalents anywhere on the planet. The uniqueness of the Noril’sk ore-bearing massifs within the extensive class of magmatic Pt–Cu–Ni deposits (the setting of the Noril’sk massifs in the world’s largest Siberian flood basalt province, their Early Triassic age, and their combination of sulfide and low sulfide types of PGE mineralization within the same massifs) continues to attract the keen interest, in both purely theoretical and applied aspects, of several researchers. The principal relations and trends revealed in the origin of the Noril’sk deposits largely facilitate exploration for analogous ores not only in the Noril’sk district itself but also throughout the Siberian Platform and elsewhere worldwide.
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